Correction to: Geochemical and isotope evidence for mantle-derived source rock of high-K calc-alkaline I-type granites, Pernambuco–Alagoas Domain, northeastern Brazil
نویسندگان
چکیده
Unfortunately, Fig. 14 shows vectors pointing in the wrong direction.
منابع مشابه
Contamination in mafic mineral-rich calc-alkaline granites: a geochemical and Sr-Nd isotope study of the Neoproterozoic Piedade Granite, SE Brazil.
The Piedade Granite (approximately 600 Ma) was emplaced shortly after the main phase of granite magmatism in the Agudos Grandes batholith, Apiaí-Guaxupé Terrane, SE Brazil. Its main units are: mafic mineral-rich porphyritic granites forming the border (peraluminous muscovite-biotite granodiorite-monzogranite MBmg unit) and core (metaluminous titanite-bearing biotite monzogranite BmgT unit) and ...
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ژورنال
عنوان ژورنال: International Journal of Earth Sciences
سال: 2021
ISSN: ['1437-3254', '1437-3262']
DOI: https://doi.org/10.1007/s00531-021-02049-1